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首页> 外文期刊>The Astrophysical journal >Evidence of a North-South Asymmetry in the Heliosphere Associated with a Southward Displacement of the Heliospheric Current Sheet
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Evidence of a North-South Asymmetry in the Heliosphere Associated with a Southward Displacement of the Heliospheric Current Sheet

机译:与日球电流表南移相关的日球南北不对称的证据

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Evidence of a north-south asymmetry in the global heliosphere, first inferred from Ulysses cosmic-ray observations, is investigated using simultaneous Ulysses and Wind magnetic field observations. Such an asymmetry, presumably associated with a southward displacement of the heliospheric current sheet (HCS), is expected to produce significantly different magnitudes of the radial field component, |BR|, in the Sun's north and south magnetic hemispheres or, alternatively, in the positive and negative magnetic sectors. Ulysses, while at high latitudes, spends time predominantly in first one and then the other hemisphere. As a consequence, measurements in the positive sector are obtained several months later than measurements made in the negative sector, making comparisons susceptible to temporal changes. To address this ambiguity, the fields in both sectors observed by the Wind spacecraft in the ecliptic were compared. A large difference in |BR| of ≈30% was observed at Wind between 1994 December and 1995 April, with |BR| larger in the south than in the north. Subsequent measurements show a gradual increase in the north (outward) radial component and a decrease in the south (inward) component, ending in only a small difference by 1995 June. Thus, the Wind observations are consistent with a southward displacement of the HCS of ≈10° and with the energetic particle observations. The secular time variation, which occurred as the spacecraft transited from the south to the north hemisphere, explains why a significant north-south difference in |BR| was not evident in the Ulysses measurements. The current sheet configuration and various questions and implications associated with these results are also discussed.
机译:首先利用尤利西斯宇宙射线观测和风磁场观测,首先从尤利西斯宇宙射线观测中推断出全球太阳圈南北不对称的证据。这种不对称性可能与日球层电流片(HCS)的向南位移有关,预计会在太阳的南北半球或北半球产生的径向场分量| BR |的大小明显不同。正负磁区。尤利西斯(Ulysses)在高纬度地区时,主要在第一半球和第二半球度过时光。结果,比在负扇区中进行的测量要晚几个月,才能获得正扇区中的测量结果,从而使比较容易受到时间变化的影响。为了解决这种模糊性,比较了风飞船在黄道中观测到的两个扇区的场。 | BR |的差异很大在1994年12月至1995年4月期间,Wind观测到约30%的| BR |。南部比北部更大。随后的测量结果显示,北(向外)的径向分量逐渐增加,而南(向内)的径向分量逐渐减小,到1995年6月只有很小的差别。因此,风的观测与HCS的南移≈10°和高能粒子观测是一致的。当航天器从南半球过渡到北半球时发生的世俗时间变化解释了为什么| BR |的南北差异显着。在尤利西斯的测量中并不明显。还讨论了当前的工作表配置以及与这些结果相关的各种问题和含义。

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